Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1111/1365-2745.13162 |
Desiccation and rehydration of mosses greatly increases resource fluxes that alter soil carbon and nitrogen cycling | |
Slate, Mandy L.1,2,5,6; Sullivan, Benjamin W.3,4; Callaway, Ragan M.1,2 | |
通讯作者 | Slate, Mandy L. |
来源期刊 | JOURNAL OF ECOLOGY
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ISSN | 0022-0477 |
EISSN | 1365-2745 |
出版年 | 2019 |
卷号 | 107期号:4页码:1767-1778 |
英文摘要 | Mosses often have positive effects on soil carbon and nitrogen cycling, but we know little about how environmentally determined cycles of desiccation and rehydration in mosses influence these processes. In this context, we compared carbon and nitrogen in throughfall after precipitation passed through eight moss species that were either hydrated continuously or desiccated and rehydrated. Also, the throughfall of four moss species was added to soil and used to determine the net effect of carbon and nitrogen added in moss throughfall on soil CO2 and N2O efflux. Depending on the species, desiccated-rehydrated (rehydrated) mosses lost 2-31 times more carbon in throughfall than mosses that were continuously hydrated (hydrated). Hydrated mosses lost little to no detectable nitrogen, whereas most rehydrated mosses lost some nitrogen in throughfall. Throughfall from both hydrated and rehydrated mosses generated higher CO2 and N2O efflux than water treated soils, but rehydrated moss throughfall promoted larger N2O efflux than hydrated moss throughfall. Throughfall from hydrated mosses caused net negative changes in soil carbon and had very little effect on soil nitrogen, whereas throughfall from rehydrated mosses generated positive changes in soil carbon and nitrogen. Synthesis. Our results indicate that resources lost from desiccated mosses during rehydration influence soil carbon and nitrogen transformations and may be important drivers of carbon and nitrogen cycling and storage in ecosystems. |
英文关键词 | bryophyte carbon storage and loss ecosystem function moss nitrogen storage and loss throughfall |
类型 | Article |
语种 | 英语 |
国家 | USA |
开放获取类型 | Bronze |
收录类别 | SCI-E |
WOS记录号 | WOS:000473096200018 |
WOS关键词 | RAIN-FOREST ; TEMPERATE DESERT ; ORGANIC-MATTER ; PULSE RELEASE ; BIOTIC CRUST ; BRYOPHYTES ; TOLERANCE ; OXIDE ; MINERALIZATION ; DYNAMICS |
WOS类目 | Plant Sciences ; Ecology |
WOS研究方向 | Plant Sciences ; Environmental Sciences & Ecology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/216933 |
作者单位 | 1.Univ Montana, Div Biol Sci, Missoula, MT 59812 USA; 2.Univ Montana, Inst Ecosyst, Missoula, MT 59812 USA; 3.Univ Nevada, Dept Nat Resources & Environm Sci, Reno, NV 89557 USA; 4.Univ Nevada, Global Water Ctr, Reno, NV 89557 USA; 5.US Forest Serv, Rocky Mt Res Stn, Missoula, MT 59801 USA; 6.MPG Ranch, Florence, MT 59833 USA |
推荐引用方式 GB/T 7714 | Slate, Mandy L.,Sullivan, Benjamin W.,Callaway, Ragan M.. Desiccation and rehydration of mosses greatly increases resource fluxes that alter soil carbon and nitrogen cycling[J],2019,107(4):1767-1778. |
APA | Slate, Mandy L.,Sullivan, Benjamin W.,&Callaway, Ragan M..(2019).Desiccation and rehydration of mosses greatly increases resource fluxes that alter soil carbon and nitrogen cycling.JOURNAL OF ECOLOGY,107(4),1767-1778. |
MLA | Slate, Mandy L.,et al."Desiccation and rehydration of mosses greatly increases resource fluxes that alter soil carbon and nitrogen cycling".JOURNAL OF ECOLOGY 107.4(2019):1767-1778. |
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